Download Volcanoes and Igneous Activity Earth - Chapter 4

Earth Science, 13e
Tarbuck & Lutgens
© 2012 Pearson Education, Inc.
POD #65
Geology of the Grand Canyon Notes
(Min. 10)
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POD # 64
1. How old is the “Blue Beauty”? ______
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POD # 64
1. How old is the “Blue Beauty”? ______
2. Video notes
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Historical notes
Catastrophism
• Landscape developed by catastrophes
• James Ussher, mid-1600s, concluded
Earth was only a few thousand years old
Modern geology
• Uniformitarianism
• Fundamental principle of geology
• “The present is the key to the past”
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Historical notes
Modern geology
• James Hutton
• Theory of the Earth
• Published in the late 1700s
• Argued that mountains are
Destroyed by weathering
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Relative dating
Placing rocks and events in sequence
Principles and rules of
• Law of superposition – oldest rocks are
on the bottom
• Principle of original horizontality –
sediment is deposited horizontally
• Principle of cross-cutting relationships –
younger feature cuts through an older
feature
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Superposition is well illustrated
in the Grand Canyon
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Cross-cutting relationships
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Relative dating
Principles and rules of
• Inclusions – one rock contained within
another (rock containing the inclusions is
younger)
• Unconformities
• An unconformity is a break in the rock record
• Types of unconformities
• Angular unconformity – tilted rocks are overlain
by flat-lying rocks
• Disconformity – strata on either side are parallel
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Formation of an Unconformity
http://www.classzone.com/books/earth
_science/terc/content/visualizations/es
2902/es2902page01.cfm?chapter_no=vi
sualization
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Formation of
an angular
unconformity
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Relative dating
Principles and rules of
• Unconformities
• Types of unconformities
• Nonconformity
• Metamorphic or igneous rocks below
• Younger sedimentary rocks above
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Several unconformities are
present in the Grand Canyon
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POD #66
**Read pages 330-332 to learn about
correlation.
1. What is the goal of correlation?
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Correlation of rock layers
Matching rocks of similar age in
different regions
Often relies upon fossils
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POD #68
1. Describe how this fossil was
formed.
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Fossils: evidence of past life
Remains or traces of prehistoric life
Types of fossils
• Petrified – cavities and pores are filled with
precipitated mineral matter
• Formed by replacement – cell material is
removed and replaced with mineral matter
• Mold – shell or other structure is buried
and then dissolved by underground water
• Cast – hollow space of a mold is filled with
mineral matter
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Fossils: evidence of past life
Types of fossils
• Carbonization – organic matter becomes a
thin residue of carbon
• Impression – replica of the fossil’s surface
preserved in fine-grained sediment
• Preservation in amber – hardened resin of
ancient trees surrounds an organism
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Cast and mold of a trilobite
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Fossils: evidence of past life
Types of fossils
• Indirect evidence includes
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Tracks
Burrows
Coprolites – fossil dung and stomach contents
Gastroliths – stomach stones used to grind
food by some extinct reptiles
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Fossils: evidence of past life
Conditions favoring preservation
• Rapid burial
• Possession of hard parts
Fossils and correlation
• Principle of fossil succession
• Fossils succeed one another in a definite and
determinable order
• Proposed by William Smith – late 1700s and
early 1800s
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Determining the ages of
rocks using fossils
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Fossils: evidence of past life
Fossils and correlation
• Index fossils
• Widespread geographically
• Existed for a short range of geologic time
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Radioactivity and
radiometric dating
Atomic structure reviewed
• Nucleus
• Protons – positively charged
• Neutrons
• Neutral charge
• Protons and electrons combined
• Orbiting the nucleus are electrons –
negative electrical charges
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POD #69
1. What did you learn from the
Radiometric Dating Lab?
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Radioactivity and
radiometric dating
Atomic structure reviewed
• Atomic number
• An element’s identifying number
• Number of protons in the atom’s nucleus
• Mass number
• Number of protons plus (added to) the
number of neutrons in an atom’s nucleus
• Isotope
• Variant of the same parent atom
• Different number of neutrons and mass
number
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Radioactivity and
radiometric dating
Radioactivity
• Spontaneous breaking apart (decay) of
atomic nuclei
• Radioactive decay
• Parent – an unstable isotope
• Daughter products – isotopes formed from
the decay of a parent
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Radioactivity and
radiometric dating
Radioactivity
• Radioactive decay
• Types of radioactive decay
• Alpha emission
• Beta emission
• Electron capture
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Types of radioactive decay
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Radioactivity and
radiometric dating
Radiometric dating
• Half-life – the time for one-half of the
radioactive nuclei to decay
• Requires a closed system
• Cross-checks are used for accuracy
• Complex procedure
• Yields numerical dates
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The radioactive decay curve
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Dating sedimentary strata
using radiometric dating
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Radioactivity and
radiometric dating
Carbon-14 dating
• Half-life of only 5730 years
• Used to date very recent events
• Carbon-14 produced in upper atmosphere
• Incorporated into carbon dioxide
• Absorbed by living matter
• Useful tool for anthropologists,
archeologists, historians, and geologists
who study very recent Earth history
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Geologic time scale
Divides geologic history into units
Originally created using relative
dates
Subdivisions
• Eon
• Greatest expanse of time
• Four eons
• Phanerozoic (“visible life”) – the most
recent eon
• Proterozoic
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Geologic time scale
Subdivisions
• Eon
• Four eons
• Archean
• Hadean – the oldest eon
• Era
• Subdivision of an eon
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Geologic time scale
Subdivisions
• Era
• Eras of the Phanerozoic eon
• Cenozoic (“recent life”)
• Mesozoic (“middle life”)
• Paleozoic (“ancient life”)
• Eras are subdivided into periods
• Periods are subdivided into epochs
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The geologic time scale
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Geologic time scale
Difficulties in dating the time scale
• Not all rocks are datable (sedimentary
ages are rarely reliable)
• Materials are often used to bracket
events and arrive at ages
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End of Chapter 11
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